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Local winds differ from global winds because they
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
The freezing point of pure water on the Celsius scale is
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
Most of the heating of the troposphere comes from
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
Heat from the sun reaches you by
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
Very high feathery clouds are called
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
Convection takes place because
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
On average, a snowfall of 20 centimeters would equal a rainfall of
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
The horse latitudes are located
convection.
radiation.
0В°C.
at about 30 degrees north and south latitudes.
2 centimeters.
cirrus clouds.
cold air is more dense than warm air.
are caused by unequal heating within a small area.
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